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5) Types of Boundaries
5) Types of Boundaries

... has folded into a huge mountain range The edge of the oceanic plate has bent downward and dug deep into the Earth and melts The melted rock rises up through the continental plate, causing more earthquakes and forming volcanic eruptions where it finally reaches the surface. An oceanic trench is a con ...
Rock Cycle PPT
Rock Cycle PPT

... Igneous rocks are formed when molten rock (magma) cools and solidifies, with or without crystallization, either below the surface as intrusive rocks or on the surface as extrusive (volcanic) rocks. ...
Climate Verses Weather
Climate Verses Weather

... -The physical climate system involves the earth's atmosphere, land surfaces, and oceans, along with the snow and ice that is so prominent in much of Canada. These components interact with one another and with aspects of the earth's biosphere to determine not only the day-to-day weather, but also the ...
More Fun with plates
More Fun with plates

... this crater many little new craters are ...
Geology II.
Geology II.

... • Rock that has been formed by molten magma or lava that has hardened. (example- granite) ...
Our Changing Landforms
Our Changing Landforms

Ever Changing Earth Test Study Guide Be able to define the
Ever Changing Earth Test Study Guide Be able to define the

... Hot spot Convergent boundary Converge Divergent boundary Diverge Rift zone Buckling zone Subduction zone Transform zone ...
Plate Tectonics Review The rock at the Earth`s surface forms a
Plate Tectonics Review The rock at the Earth`s surface forms a

... These seismic waves tell us that the layers (crust, mantle, outer core, inner core) have distinct properties and composition. The interior of the Earth is hot. Convection currents- heat flow and movement of material within the Earth cause sections of Earth’s crust to move. This may result in earthqu ...
GEOL1010 Hour Exam 1 Sample
GEOL1010 Hour Exam 1 Sample

... continents and oceans? (20pts) Igneous fractionation is the process of deriving a magma of a different chemical composition from a rock of a definite composition, by partial melting and fractional crystallization. 10 points for knowing that a rock of one composition is derived from one of another co ...
GCS Earth Science Unit B Test
GCS Earth Science Unit B Test

Extraterrestrial Volcanism
Extraterrestrial Volcanism

... i.Olympus Mons is the largest of the discovered volcanos on mars. 1.It is 28km tall, 600km across at the base, and 70km across at its caldera. 2.One theory explaining why this volcano grew so large is that Mar’s crust does not drift like Earth’s. Therefore, this volcano stayed over the lava source ...
Diapositiva 1
Diapositiva 1

... to the Earth’s surface. This process is called uplift. Once exposed to the elements the rock on the Earth’s surface begins to weather and erode. The rock cycle begins all over again. RETURN ...
Unit 1: Basics of Geography Chapter 2
Unit 1: Basics of Geography Chapter 2

... either one to dive under the other or the edges of both to crumple • Transform boundary- plates slide past one another ...
Calderas Lava Plateaus
Calderas Lava Plateaus

Powerpoint Presentation Physical Geology, 10/e
Powerpoint Presentation Physical Geology, 10/e

... generally increases with increasing pressure Decompression melting can occur when hot mantle rock moves upward and pressure is reduced enough to drop melting point to the temperature of the rising rock body ...
Rock Cycle Who Wants to be a Millionaire PowerPoint
Rock Cycle Who Wants to be a Millionaire PowerPoint

... The Rock Cycle can be compared to which one of these process the closest? A – Circle of Life ...
Plate Tectonics DQ - Biloxi Public Schools
Plate Tectonics DQ - Biloxi Public Schools

... 1. Convection currents, which may be the driving force for the movement of lithospheric plates, are mostly found in Earth’s A. crust B. outer core C. plastic mantle D. inner core Justification--____________________________________________________________ _____________________________________________ ...
Global Systems - Vocabulary Worksheet File
Global Systems - Vocabulary Worksheet File

... We can consider that materials are moved or recycled through the Earth through several interconnected natural systems by natural processes. For example, an atom of oxygen will move through the biosphere through the processes of photosynthesis and respiration but will also enter the hydrosphere throu ...
S05Exam3
S05Exam3

... _____3. The largest volcanic eruptions of the last two centuries (eg. Pinatubo, Krakatau, Tambora) resulted in global: [A. cooling, B. warming, or C. no change] to climate within one to two years of the eruption. _____4. The currently accepted approximate temperature at the center of the Earth's inn ...
10024 - WeberTube
10024 - WeberTube

... the RICHTER SCALE, which measures the energy released by a quake. A 2.0 quake would not be noticed, while a 4.5 would probably be reported in the news. Major quakes are those over a 7.0.  In 1906, the quake that destroyed San Francisco was likely at least an 8.0. ...
The Wadati-Benioff Zone
The Wadati-Benioff Zone

... 4) At what horizontal location in this plot is there evidence for volcanic activity? (hint: magma movements create earthquakes) Why is there volcanic activity here? at 500 km there is evidence for volcanic activity. There is volcanic activity here because the downgoing plate has released its water d ...
Igneous Rocks and Their Origin
Igneous Rocks and Their Origin

... generally increases with increasing pressure ...
lesson 9
lesson 9

... Year: ...
Geosphere, Atmosphere, Hydrosphere, and Biosphere.
Geosphere, Atmosphere, Hydrosphere, and Biosphere.

The Rock Cycle - Union Academy
The Rock Cycle - Union Academy

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Tectonic–climatic interaction



Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect. As the geological record of past climate changes over millions of years is sparse and poorly resolved, many questions remain unresolved regarding the nature of tectonic-climate interaction, although it is an area of active research by geologists and palaeoclimatologists.
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